Modeling of Long-Period Ground Motions in the Nankai Subduction Zone: Model Simulation Using the Accretionary Prism Derived from Oceanfloor Local S-Wave Velocity Structures
Author:
Funder
Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00024-018-2013-8/fulltext.html
Reference83 articles.
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3. Archuleta, R., & Ji, C. (2016). Moment rate scaling for earthquakes 3.3 ≤ M ≤ 5.3 with implications for stress drop. Geophysical Research Letters, 43, 12004–12011. https://doi.org/10.1002/2016GL071433 .
4. Arroyo, I. G., Husen, S., Flueh, E. R., Gossler, J., Kissling, E., & Alvarado, G. E. (2009). Three-dimensional P-wave velocity structure on the shallow part of the central Costa Rican Pacific margin from local earthquake tomography using off- and onshore networks. Geophysical Journal International, 179, 827–849. https://doi.org/10.1111/j.1365-246X.2009.04342.x .
5. Asano, K., & Iwata, T. (2016). Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data. Earth, Planets and Space, 68, 147. https://doi.org/10.1186/s40623-016-0519-9 .
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